城市地下空洞等值反磁通瞬变电磁三维正演模拟及分析
Simulation and Analysis of 3D Forward Modeling of Opposing Coils Transient Electromagnetic Field in Urban Underground Cavity
DOI: 10.12677/AG.2022.121012, PDF,   
作者: 姚富宝, 王 鹤:中南大学地球科学与信息物理学院,湖南 长沙;侯海涛:中南大学地球科学与信息物理学院,湖南 长沙;湖南五维地质科技有限公司,湖南 长沙
关键词: OCTEM矢量有限元空洞响应3D正演OCTEM Vector Finite Element Void Response 3D Modeling
摘要: 等值反磁通瞬变电磁法(Opposing Coils TEM,简称OCTEM)由于具有浅层盲区小、施工效率高等优点,目前在城市浅层地球物理勘探领域受到了广泛的应用。为研究OCTEM在城市地下空洞探测中的应用,基于等值反磁通理论与矢量有限元瞬变电磁三维正演算法,构建低阻异常模型、高阻异常模型,分析了不同填充状态情况下的空洞OCTEM响应规律。并遵循相似性原则设计进行物理实验,对比数值计算和物理实验结果论证了数值模拟结果的正确性。结果表明:OCTEM对高阻异常与低阻异常都具有良好的识别能力,但对于低阻异常体OCTEM更为敏感。研究结果可为OCTEM在实际空洞探测应用中提供参考。
Abstract: The opposing coils transient electromagnetic method (OCTEM) has been widely used in the field of urban shallow geophysical exploration due to its advantages of small shallow blind area and high efficiency. In order to study the application of OCTEM in urban underground cavity detection, based on the opposing coils theory and vector finite element transient electromagnetic 3D forward algorithm, low resistance anomaly model and high resistance anomaly model were constructed, and the OCTEM response law of cavity under different filling conditions was analyzed. The physical experiment was designed according to the similarity principle, and the correctness of the numerical simulation results was verified by comparing the numerical calculation and the physical experiment results. The results show that OCTEM has good recognition ability for both high and low resistance anomalies, but is more sensitive to low resistance anomalies. The results can provide a reference for the application of OCTEM in cavity detection.
文章引用:姚富宝, 王鹤, 侯海涛. 城市地下空洞等值反磁通瞬变电磁三维正演模拟及分析[J]. 地球科学前沿, 2022, 12(1): 105-114. https://doi.org/10.12677/AG.2022.121012

参考文献

[1] 高远. 等值反磁通瞬变电磁法在城镇地质灾害调查中的应用[J]. 煤田地质与勘探, 2018, 46(3): 152-156.
[2] 王银, 席振铢, 蒋欢. 等值反磁通瞬变电磁法在探测岩溶病害中的应用[J]. 物探与化探, 2017, 41(2): 360-363.
[3] 席振铢, 龙霞, 周胜, 黄龙, 宋刚, 侯海涛, 王亮. 基于等值反磁通原理的浅层瞬变电磁法[J]. 地球物理学报, 2016, 59(9): 3428-3435.
[4] 薛国强, 李貅, 底青云. 瞬变电磁法正反演问题研究进展[J]. 地球物理学进展, 2008, 23(4): 1165-1172.
[5] 李建慧, 朱自强, 曾思红. 瞬变电磁法正演计算进展[J]. 地球物理学进展, 2012, 27(4): 1393-1400.
[6] 薛国强, 常江浩, 雷康信, 陈康. 瞬变电磁法三维模拟计算研究进展[J]. 地球科学与环境学报, 2021,43(3): 559-567.
[7] Kuo, J.T. and Cho, D.H. (1980) Transient Time-Domain Electromagneti. Geophysics, 45, 271-291. [Google Scholar] [CrossRef
[8] Gupta, P.K., Bennett, L.A. and Raiche, A.P. (1987) Hybrid Calculations of the Three-Dimensional Electromagnetic Response of Buffed Conductors. Geophysics, 52, 301-306. [Google Scholar] [CrossRef
[9] Gupta, P.K., Raiche, A.P. and Sugeng, F. (1989) Three-Dimensional Time-Domain Electromagnetic Modelling Using a Compact Finite-Element Frequency Stepping Method. Geophysical Journal International, 96, 457-468. [Google Scholar] [CrossRef
[10] 殷长春, 刘斌. 瞬变电磁法三维问题正演及激电效应特征研究[J]. 地球物理学报, 1994(S2): 486-492.
[11] 唐新功, 胡文宝, 严良俊. 多个三维薄板瞬变电磁响应的比较[J]. 江汉石油学院学报, 1999, 21(4): 57-60.
[12] Borner, R.U., Ernst, O.G. and Spitze, R.K. (2008) Fast 3-D Simulation of Transient Electromagnetic Fields by Model Reduction in the Frequency Domain Using Krylov Subspace Projection. Geophysical Journal International, 173, 766-780. [Google Scholar] [CrossRef
[13] 李建慧, 朱自强, 鲁光银, 曾思红. 回线源瞬变电磁法的三维正演研究[J]. 地球物理学进展, 2013, 28(2): 754-765.
[14] Chung, Y., Son, J.-S., Lee, T.J., Kim, H.J. and Shin, C. (2014) Three-Dimensional Modelling of Controlled-Source Electromagnetic Surveys Using an Edge Finite-Element Method with a Direct Solver. Geophysical Prospecting, 62, 1468- 1483. [Google Scholar] [CrossRef
[15] 李瑞雪, 王鹤, 席振铢, 蒋欢, 刘愿愿. 瞬变电磁快速三维正演[J]. 中南大学学报(自然科学版), 2016, 47(10): 3477-3482.
[16] 马炳镇. 起伏地形下地面瞬变电磁法三维正演数值模拟研究[J]. 物探与化探, 2018, 42(4): 777-784.
[17] 张永超, 李宏杰, 邱浩, 廉玉广, 李文. 矿井瞬变电磁法的时域矢量有限元三维正演[J]. 煤炭学报, 2019, 44(8): 2361-2368.
[18] 李瑞雪, 席振铢, 周胜, 宋刚. 深海热液金属硫化物矿瞬变电磁响应的三维正演模拟[M]. 长沙: 中南大学出版社, 2007.
[19] Nabighian, M.N. and Macnae, J.C. (1991). Time Domain Electromagnetic Prospecting Methods. Investigations in Geophysics, 2, 427-520.[CrossRef